Albedo = Fractional reflectance SurfaceAlbedo % Perfect100 Fresh snow80-90 Old snow45-70 Clouds 300-600 m thick59-84 Clouds 150-300 m thick45-75.

Slides:



Advertisements
Similar presentations
What is an Urban Heat Island? Just from the name of this term, make a guess at what it means. Write the answer in your green book.
Advertisements

Global Warming By Charlotte Bootherstone.
1 © 2010 Ronnen Levinson Ronnen Levinson, Ph.D. Acting Leader, Heat Island Group Environmental Energy Technologies Division Lawrence.
/14 Term project 2006 Definition of Urban Heat Island and it’s mechanism Department of Civil and Environmental System Engineering University.
Photosynthesis and Light
Earth Systems and Patterns: SC.5.E.7.3
1 © Heat Island Group – Lawrence Berkeley National Laboratory Cool Pavements for Cool Communities August 1, 2013 Heat Island Group.
How Does Heat Energy Travel and Insolation
Earth Science Topic #5 &6 Review Game
Chapter 17 Study Guide Answers
Green Roof Technology By: Abby Roemer. Did you know… America's 81 million buildings consume more energy than any other sector of the U.S. economy, including.
The Roof Garden Initiative of the City of New York Promoting health, leisure, and environmental friendliness on a metropolitan scale.
(Terrestrial) Planetary Atmospheres I.  Atmosphere: ◦ Layer of gas that surrounds a world  Thin for terrestrial planets ◦ 2/3 of air within 10 km of.
Seasons Why we have them And some local effects. The Earth tilts The Earth travels around the sun in an ellipse –The tilt of the North of the Earth is.
Urban Heat Island. Air temperature measurements: Thermometer is located in the shade at about 1.5 meters above a short grass surface in an open field.
Radiation Heat Transfer. The third method of heat transfer How does heat energy get from the Sun to the Earth? There are no particles between the Sun.
Chapter 2: Weather Factors
MITIGATING CLIMATE CHANGE. WHAT WE KNOW The level of greenhouse gases in the atmosphere have increased, causing the Earth’s temperature to rise. One greenhouse.
Quick Review: El Nino & La Nina
Cool Cities, CITRIS Mini-conference Feb. 25, 2011 White Roofs to Cool your Buildings, and Cities and (this is new) Cool our Planet Arthur H. Rosenfeld,
San Antonio “Hot Islands” Sandra Ytuarte December 1, 2004 Noreen Castellano.
Urban Changes & Climate
Atmosphere and Climate Change
9/10/20151 Climate & Calculating BTU’s in Environmental Science By Dr. Rick Woodward.
“Chicago Climate Jeopardy” Directions: Click on one of the numbered hyperlinks on the next slide. The hyperlink will take you to the question slide. Then,
Low Carbon Cities: Ecological processes in the eThekwini Open Space system Bob Scholes 4 October 2010.
What is climate change? Climate change is the change in long-term weather patterns in certain regions. These changes can affect the entire Earth.
Ecology & Environmental Problems Ron Chesser Urban Ecology Chapters 6, 27.
Albedo: Its effects on global warming in Polar Regions Presented by Morton Sternheim.
CLIMATE SYSTEM AND WEATHER. WEATHER Weather refers to: The state of the atmosphere in a particular place and time. Weather occurs over short time periods.
Explain what this picture shows. (your definition of heat island)
Climate Chapter 25. Climate – the average weather conditions of an area over a long period of time –But weather is the day to day conditions Climate you.
Cool Roofs: From Cool Cities to a Cooler World Arthur H. Rosenfeld, Commissioner California Energy Commission (916)
Can Green Roofs Help Mitigate the Urban Heat Island Effect?
Welcome Back Write down the 4 layers of the atmosphere (in order) and 1 fact about each.
 Introduction  Surface Albedo  Albedo on different surfaces  Seasonal change in albedo  Aerosol radiative forcing  Spectrometer (measure the surface.
Air Quality of NY By: Siré Bah and Stanley Mei. Why is Air Quality Important? O.o Why is Air Quality Important? O.o ♦ It is part of your everyday life.
El niño / La niña. Volcanic eruptions: release tiny ash particles into atmosphere which can block solar radiation and cool the planet Eruptions & Cimate.
The Atmosphere: Energy Transfer & Properties Weather Unit Science 10.
Energy in the Atmosphere
 There are two common meanings of the term "greenhouse effect". There is a "natural" greenhouse effect that keeps the Earth's climate warm and habitable.
Heat in the Atmosphere The sun’s energy is transferred to earth and the atmosphere three ways Radiation, Convection and Conduction.
Warmup How does deforestation affect our climate? How do you calculate your carbon footprint?
Active Solar heating Used for space and or water heating
Global Warming By: Majed Al Naimi 8D. Define Global warming is when the earth heats up (the temperature rises). It happens when greenhouse gases (carbon.
Solar Unit. More vocab from Nova – Saved by the Sun Greenhouse gas – Gases that can absorb and emit infrared radiation.infrared radiation By their percentage.
Green House Effect and Global Warming. Do you believe that the planet is warming? 1.Yes 2.No.
Global Warming Learning goal: determine the long term impact of humans on weather and vise versa.
1 Definition of Urban Heat Island and it’s mechanism Department of Civil and Environmental System Engineering University of Incheon, South Korea Chi-Man,
Insolation INcoming SOLar radiATION Strength is dependent on 1.Angle of insolation 2.Duration of insolation 3.Type of surface receiving the insolation.
1 White Roofs to Cool the World---- Update and Recommendations Rosenfeld Symposium UC Davis EE Center March 9, 2010 Arthur H. Rosenfeld, Former Commissioner.
Urban Heat Islands and Mitigation Strategies
Warmup What is the Industrial Revolution? How does it relate to climate change?
Balance of Energy on Earth Yumna Sarah Maria. The global energy balance is the balance between incoming energy from the sun and outgoing heat from the.
Challenges in Green development, Myanmar Chaw Kalyar Green Building Committee Building Engineering Institute 19 Nov 2015.
ENERGY IN ECOSYSTEMS Chapter The sun is the source of all energy for the earth and its ecosystems. What happens to the suns energy? What is it used.
Chapter 17 Study Guide Answers
Heat Transfer in the Atmosphere
ALBEDO ability of a surface to reflect light & heat energy back into the atmosphere & space Low Medium High anything darker / black anything middle spectrum.
Warmup How does deforestation affect our climate?
Energy in the Earth’s Atmosphere
A Science Sisters Presentation.
FIGURE 2.1 Comparison of Kelvin, Celsius, and Fahrenheit scales.
Making and Breaking of Heat Islands
Heat Islands 2.6.3B EXPLAIN HOW LARGE-SCALE DEVELOPMENT CONTRIBUTES TO REGIONAL CHANGES IN CLIMATE (I.E. HEAT ISLANDS IN LARGE CITIES LIKE NY, CHICAGO,
Angle of Incidence The shape of the Earth also plays a part in insolation. Because it’s spherical, a light ray hitting at the equator strikes the Earth.
The global energy household
Warmup How does deforestation affect our climate?
Do Now Please have out any information pertaining to heat islands as we will be discussing them today to prepare for your engineering design challenge.
ECONOMIC INCENTIVES FOR
Presentation transcript:

Albedo = Fractional reflectance SurfaceAlbedo % Perfect100 Fresh snow80-90 Old snow45-70 Clouds m thick59-84 Clouds m thick45-75 Clouds < 150 m thick25-63 Clouds (average)50-55 Sea ice30-40 Desert25-30 Grassland16-20 Green leaves5-25 Green forest5-10 Water5-10 Concrete17-27 bare ground15 Average road12 Bitumen road5-10 Freshly paved road~4 Charcoal4 no reflection0

MaterialAlbedoEmissivity Concrete Red Brick Tar Paper White Plaster Bright Galvanized Iron Bright Aluminum Foil White Pigment White Single-Ply Roofing* Black EPDM Roofing* Gray Pigment Green Pigment White Paint on Aluminum Black Paint on Aluminum Aluminum Paint – 0.67 Gravel

Sacramento Night-time temperatures June 29, White is hottest, followed by red. Blue is coolest

Heat Wave of July 1995 – 526 dead in Chicago average max 4 days 101F Heat Wave of July 1999 – 232 dead in 9 State Area 127 in Illinois, predominately Chicago average max 4 days 97 F, shorter duration, better Public health

The heat wave in July 1995 in Chicago was one of the worst weather-related disasters in Illinois history with approximately 525 deaths over a 5-day period. As noted by Changnon et al. (1996), "The loss of human life in hot spells in summer exceeds that caused by all other weather events in the United States combined, including lightning, rainstorms/floods, hurricanes, and tornadoes." Weather hazards such as tornadoes, floods, lightning, and winter storms each result in about 100 deaths per year on average, while heat waves result in about 1000 deaths per year on average.

A Social Autopsy of Disaster inChicago Heat Wave Eric Klinenberg

Climatology of Midwest Heat Wave of 1999 (Plaecki and Changnon, UIUC) 80% Deaths Night time cooling minimal

Planting and higher density ballast are estimated to decrease the amount of direct sun on the total roof by 25%. The design of the rooftop garden is intended to retain and utilize the maximum amount of water needed for the plants. In order to ensure plant viability throughout the summer, the green roof's semi-intensive and intensive zones will be irrigated as necessary to ensure that the vegetation receives enough water. The projected avoided energy cost is $3,600 per year. The total direct savings are estimated to be 9,272 kWhr per year and the corresponding savings in natural gas for heating are 7,372 therms per year.

Light-colored roofing is a time-honored method of lowering the temperature of a building. Since the advent of air conditioning this strategy has been largely ignored. On average, 17% of our urban landscape is covered with dark asphalt shingled roofs. This means that more than 60% of the rooftops are dark colored. Dark rooftops absorb and radiate heat causing outdoor air temperatures to rise, thus adding to the Urban Heat Island effect. Using light colored roofing materials or reflective coatings lower indoor and surrounding temperatures, which reduces smog. It will not make your home colder in the winter. The winter time sun is too low in the sky and too weak to provide much heating benefit to your home. One way to measure the amount of heat reflected is by calculating the albedo or solar reflectance of a roof material. Tree Facts: A single mature, properly watered tree with a crown of 30 feet can "evapotranspire" up to 40 gallons of water in a day, which is like removing all the heat produced in four hours by a small electric space heater. One large, mature sugar maple can sequester 450 pounds of carbon from the atmosphere. Twenty-nine such trees remove the CO2 generated by a car; one tree absorbs the CO2 produced by a car over 26,000 miles

Good High albedo High emissivity

Paving Materials for Heat Island Mitigation M. Pomerantz, H. Taha, A. Chen,* A. RosenfeldÝ *Center for Building Science, Energy & Environment Division, LBNL. ÝSenior Advisor for Energy Efficiency, Office of Energy Efficiency & Renewable Energy, U.S. DOE. One of the causes of higher temperatures in cities (compared to their environs) is the absorption of sunlight by dark pavements. In warm climates, this absorption can contribute damage to the environment by adding to air-conditioning electrical demand and smog. In this work, the dollar value of potential savings from lighter pavements is estimated. We examined the effect of paving urban roads, driveways, and walkways with materials that are lighter colored than black asphalt. The lighter color means that the sunlight is reflected rather than absorbed, and so the pavement is cooler. If a pavement is cooler, its lifetime is longer and the environmental damage of disposing of it is lessened. Reflectivity is also a safety factor in visibility at night, and this factor reduces the demand for electric lighting for streets. The drawback of high reflectivity is glare, which may be a limiting consideration. We considered new pavements, which are made of cement concrete; more flexible surfaces, like asphalt concrete; and porous pavements, such as grass pavers. We also reviewed materials for resurfacing existing pavements. We assembled information on the compositions of the materials, their suitabilities for particular applications, and their approximate costs.

We have shown by computer simulation that, if all possible pavements were whitened to an albedo of 0.35, the cooling of the city would save electricity and reduce smog damage. The present dollar value of these savings in Los Angeles is estimated to be $1.80/m2 ($0.17/ft2) of pavement. The cost of pavement depends on the amount of material used. If the surface layer is thin enough, its cost may be sufficiently low that the savings from a lighter color would pay for any extra cost. Thus, it may happen that a lighter pavement is overall less costly than a dark one. We illustrate this in the Figure. If the savings is $1.80/m2, for a 6-mm (1/4-in.) thick resurfacing, money would be saved, as long as the extra costs of the aggregate and binder are within the triangle to the left of the filled squares. For example, an increase of binder price by $1.64 per liter ($6.25 per gallon) and no increase in aggregate price will not increase the pavement cost more than $1.80/m2. Or, aggregate priced at $138 per Mg ($126 per ton) more than present cost, and no increase in binder price, could be used without exceeding the benefits of the cooler surface. Such aggregate can be quite white and yield a more reflective surface, with no overall extra cost to society. If the pavement is 25 mm (1 in.) thick, the range of affordable price increases is confined to the area below the line defined by the open squares. The four times thicker surface implies a four times smaller range of affordable price increases.

Fall 2001, Alderman Mary Ann Smith 48 th. Gravelpave2, porous structure In 40x40 inche square 144 rings 2 in diameter 1 inhigh, held together by Geofabric layer. Handles up to 3”/hour rainfall without connecting to sewers City of Chicago Web Site, DOE

Loyola’s New Life Science Building Roof 3= Green Env. Seminar Series Fall 2000 Injected Idea of Green roof Into the design